Lewis Owen has been
                                    scraping out icy fragments of history’s truth from one of the most glaciated
                                    regions on Earth for the past 25 years. His frequent excursions to Tibet and
                                    the Himalayas have led the University of Cincinnati professor of geology to
                                    some cold, hard facts. Owen knows climate change
                                    is immortal — fluctuating across millennia, patiently building toward moments
                                    when circumstances are ripe for apocalypse. It was true thousands of years ago,
                                    when rapid climate change had profound effects on landscapes and the creatures
                                    that lived on them. That scenario could be true again, if the past is ignored. 
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“We’re interested in
                                    how glaciers change over time as climate has changed, because we’re in a
                                    changing climate at the moment, dominantly because of increased human
                                    activity,” Owen says. “From
                                    understanding past glacial changes, we can understand how glaciers may change
                                    in the future.” 
Owen, head of UC’s
                                    Department of Geology, is among a team of researchers at the university who
                                    have been gathering and studying years of data on Tibet and the Himalayas.
                                    Members of the group contributed to two research papers that will be published
                                    in the March 15 edition (Vol. 88) of Quaternary Science Reviews, an
                                    international, multidisciplinary research and review journal.
BIG DIFFERENCES IN HUGE
                                    GLACIERS
Glaciers are fickle beasts.
                                    They don’t all respond to climate change in the same way. Some recede while
                                    others surge, and these changes can have a profound effect on landscapes — at
                                    times to dangerous effect. Glacial lakes, which swell as glaciers melt, can
                                    drain in catastrophic fashion, known as glacial lake flood outburst. Owen says consequences of such outbursts can be severe,
                                    wiping out entire villages or ruining acres of farmland. Comparing glacial
                                    areas and anticipating melt is a complex problem but one that underscores the
                                    importance of his research, Owen says. 
“Glaciers will vary
                                    from one side of the mountain range to the next very differently. As part of
                                    our research, we’re building up a standard scheme that people can use to
                                    compare their glaciated areas,” Owen says.
The environmental stakes
                                    are as high as the mountains themselves. Tibet and the Himalayas are nearly
                                    one-third the size of the contiguous 48 U.S. states, and nearly a billion
                                    people live in the mountains’ shadow. Waters from the glaciers flow into the
                                    Indo-Gangetic Plain, a fertile region including parts of Bangladesh, India,
                                    Nepal and Pakistan, and bordered to the north by China. The source water for
                                    some of the world’s largest rivers — the Indus, Ganges, Yangtze and Yellow — is
                                    derived from these glaciers.
Read more at the University of Cincinnati
                                    News.
Mountains-scape
                                    in Everest National Park image via Shutterstock.



